3 edition of Data report for 1980-1981 seismic-refraction profiles in the western Mojave Desert, California found in the catalog.
Data report for 1980-1981 seismic-refraction profiles in the western Mojave Desert, California
1988 by Dept. of the Interior, U.S. Geological Survey, [Books and Open-File Reports Section, distributor] in [Denver, Colo.?] .
Written in English
|Statement||by R.N. Harris, A.W. Walter and G.S. Fuis.|
|Series||Open-file report -- 88-580, U.S. Geological Survey open-file report -- 88-580..|
|Contributions||Walter, A. W., Fuis, Gary S., Geological Survey (U.S.)|
|The Physical Object|
Bulletin of the Seismological Society of America, Vol. 75, No. 1, pp. , February A SEISMIC-REFRACTION PROFILE ACROSS THE SAN ANDREAS, SARGENT, AND CALAVERAS FAULTS, WEST-CENTRAL CALIFORNIA BY WALTER D. MOONEY AND ROBERT H. COLBURN ABSTRACTFile Size: 1MB. Mineral impact study of a 2, square mile area of the East Mojave Desert, San Bernardino County, California by Evans, J. R; California State Mining and Geology Board; California. Division of Mines and Geology; United States. Bureau of Land : Huntington Beach is a seaside city in Orange County in Southern California, located 35 miles southeast of Downtown Los city is named after American businessman Henry E. population was , during the census, making it the most populous beach city in Orange County and the seventh most populous city in the Los Angeles-Long Beach-Anaheim, CA Metropolitan Country: United States. Sarah Bridge. Phoenix, Arizona Area Licensed Clinical Social Worker in Private Practice Individual & Family Services Education University of Southern California — Masters of Social Work University of California, Los Angeles — B.A., Psychology Experience Sarah Bridge LLC - Present The Meadows of Wickenburg - Present Center Against Sexual Abuse (CASA), a non /5(73).
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During andthe U.S. Geological Survey collected seismic refraction data in the western Mojave Desert (fig. The seismic refraction data extends from north of the Garlock Fault, south through the Mojave Desert, and across the San Andreas Fault into the San Gabriel by: 1.
Abstract. A U.S. Geological Survey report is presented containing data for seismic-refraction profiles in the western Mojave Desert, California.
During andthe USGS collected seismic refraction data in the western Mojave Desert. The seismic refraction data extends from north of the Garlock Falult, south through the Mojave Desert, and across the San Andreas Fault into the San Gabriel Montains.
Data report for seismic-refraction profiles in the western Mojave Desert, California. Stanford Libraries' official online search tool for books, media, journals, databases, government documents and more.
Buy Data report for seismic-refraction profiles in the western Mojave Desert, California (Open-file report / Department of the Interior, U.S.
Geological Survey) by Harris, R. N (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : R. N Harris. PDF | On Jan 1,J. Trijonis and others published RESOLVE project: Visibility conditions and causes of visibility degradation in the Mojave Desert of California | Find, read and cite all the.
Seismic and gravity data taken along line 1 of the Consortium for Continental Reflection Profiling (COCORP) Mojave Desert Survey (N-S profile, km long) have been used to characterize the upper crust north of the San Andreas fault in the western Mojave block of southern California.
A 2-D upper crustal structural profile with seven steeply dipping faults was constructed from the Los Angeles Region Seismic Experiment phase II (LARSE II) seismic refraction data recorded over the north central Transverse ranges and adjacent Mojave desert in southern California.
The profile extends to a depth of approximately 4 by: Download Citation | Seismic refraction evidence for steep faults cutting highly attenuated continental basement in the central Transverse ranges, California | A 2-D upper crustal structural. The valley is a granitic basin filled with unconsolidated material.
In August and June and Julythe U.S. Geological Survey conducted a seismic- refraction survey consisting of four lines northwest of the valley, eight lines in the valley, and six lines northeast of the : L.F.
Duell. Data report for a seismic-refraction investigation: Morro Bay to the Sierra Nevada, California (Open-file report / United States Department of the Interior, Geological Survey) [J.
M Murphy] on *FREE* shipping on qualifying offers. Colburn, R. and Walter, A. (), Data report for two seismic-refraction profiles crossing the epicentral region of the Coalinga, California earthquakes, U.S.G.S. Open-File Report Cited by: 3. Seismic data from a km-long refraction profile in the Santa Barbara Channel have been interpreted using several velocity inversion techniques.
Data were obtained during two cruises in and Cited by: Tectonophysics, In the U.S. Geological Survey collected six seismic refraction profiles in the Great Valley of California: three axial profiles with a maximum shot-to-receiver offset of km, and three shorter profiles perpendicular to the valley axis.
Six of the seven faults detected from the seismic data correspond directly to geologically mapped faults in the central Transverse ranges and adjacent Mojave desert.
From south to north, they are the Pelona fault, the San Francisquito fault, the Clearwater fault, the San Andreas fault and two faults that cut the Portal ridge. The seventh fault is buried beneath Quaternary deposits of the western Mojave desert.
The Moho is relatively flat at the average depth in the western and central Mojave Desert and becomes shallower to the east under the Eastern California Shear Zone (ECSZ). Southern California crust has an average V_p/V_s ratio ofwith higher ratios of to in the mountain ranges with Mesozoic basement and lower ratios in the Mojave Cited by: If your FDSN web service is not listed, or you plan to distribute data via some other method, or you do not plan to distribute data, please provide details below.
Data distribution notes Data converted from original SEGY archived data from report into PH5 as part of an effort to make historical data visible to the public in ph5 format. The U.S. Department of Energy's Office of Scientific and Technical Information.
General Information. Title: Simplified geologic map of the western Mojave Desert, California Author(s): Dibblee, T.W. Publishing Organization: U.S. Geological Survey Series and Number: Open-File Report OF Publication Date: Map Scale:Cross Section: None North Latitude: 35° 34' 5" N () South Latitude: 34° 9' 40" N () East Longitude: ° 0' 0" W ().
Igneous dikes buried beneath as much as 2 m of alluvium in the Mojave Desert of California were detected by the SEASAT L-band (cm wavelength) synthetic-aperture radar (SAR) in The roughness and dihedral configuration of the dikes are favorable to generation of strong radar by: The primary purpose of this report and the geologic map is to provide a geologic background for the exploration for possible concealed borate deposits in the western Mojave Desert, based upon (1) the geology of the known deposits of these minerals within the region, (2) the areal geology of the region, and (3) the subsurface geology as determined insofar as possible from logs of exploratory test holes, mine workings Author: U.S.
Department of the Interior. Compressional- (P-) wave seismic refraction data were acquired in December and July along fourteen profiles within the spillway of Success Dam in Porterville, California. A new concrete ogee weir is planned for construction within the existing spillway, and the P-wave seismic velocity models will be used to inform further geotechnical.
The study site is at an elevation of m, approximately 22 km south of Baker, California and km southwest of Las Vegas, selected basalt flow, mapped as the e1 flow (Dohrenwend et al., ), was chosen because it allows the study of surficial processes on a desert pavement whose lithology (basalt) and time of development (,±, years; Turrin et al., ) are by: A Preliminary Report of a Rock Feature Complex on the East Side of Searles Lake (CA-SBR/H), Western Mojave Desert, San Bernardino County, California [PCASQ - PDF].
Laylander, Don Click on the book chapter title to read more. Crustal reflectivity from the Santa Monica Mts to the western Mojave Desert, from the Los Angeles Region Seismic Experiment (Phase II), southern California Trond Ryberg, Gary S.
Fuis, William J. Lutter, & Klaus Bauer In PreparationSCEC Contribution # sin in Antelope Valley, Mojave Desert, California (Figure 1), where the U.S. Geological Survey has been collecting geohy-drologic and geodetic data for many decades.
The interfero-gram was originally developed by the Jet Propulsion Labora-tory (JPL) to study crustal deformation in the Los Angeles area and along the San Andreas Size: 2MB. ABSTRACT LUMINESCENCE DATING OF CERAMICS FROM ARCHAEOLOGICAL SITES IN THE SODA LAKE REGION OF THE MOJAVE DESERT By Andrea C.
Bardsley August Ceramic studies in the Mojave Desert of California have long been plagued with vague and imprecise chronological data and have relied heavily on relative dating. Recovery of secular deformation ﬁeld of Mojave Shear Zone in Southern California from historical terrestrial and GPS measurements Shaozhuo Liu1, Zheng-Kang Shen2,3, and Roland Bürgmann4 1State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing, China, 2Departmentof Earth, Planetary,andSpaceSciences, University ofCalifornia,LosAngeles.
Table 1. Summary of wells with data used in this report by type and well depth, Mojave River and Morongo groundwater basins, Southwestern Mojave Desert, San Bernardino County, California, [ft, feet;, actual value is greater than value shown] Well Type Number of Well Sites (Sampling Points) 1.
Seismic-refraction profiles recorded north of Mammoth Lakes, California, using earthquake sources from the January swarm complement earlier explosion refraction profiles and provide velocity information from deeper in the crust in the area of the Long Valley caldera.
Eight earthquakes from a depth range of 4. 9 to 8. 0 km confirm the observation of basement rocks with seismic velocities. The primary purpose of this report and the geologic map is to provide a geologic background for the exploration for possible concealed borate deposits in the western Mojave Desert, based upon (1) the geology of the known deposits of these minerals within the region, (2) the areal geology of the region, and (3) the subsurface geology as determined Pages: Water resources data for California, Part 2, water quality records.
U.S. Geological Survey,Water resources data for California, annual data report, part 1, surface water records, v. 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley: Water Data Report.
U.S. Geological Survey, Data report for the Los Angeles region seismic experiment (LARSE93), Southern California; a passive study from Seal Beach northeastward through the Mojave Desert Open-File Report 2.
Characteristics of Lavic Siding Pavement Study Site  The Hector Mine earthquake [U.S. Geological Survey et al., ] occurred 16 October in the Mojave Desert about 80 km east‐southeast of Barstow, California, and within the boundaries of Twentynine Palms Marine Corps Base ().Field observations reported below were carried out from 30 October through 1 November Cited by: 7.
A Preliminary Report of a Rock Feature Complex on the East Side of Searles Lake (CA-SBR/H), Western Mojave Desert, San Bernardino County, California Kish D. La Pierre Abstract Nothing stands out on the archaeological landscape (quite literally) like architecture in demonstrating variability and adaptation to a given environment.
Aeolian responses to climate variability during the past century on Mesquite Lake Playa, Mojave Desert. The erosion and deposition of sediments by wind from to have created large changes in surface features of Mesquite Lake playa in the Mojave Desert. Geology and plate-tectonic development: 4.
Quaternary deformation: 5. Seismicity, 6. Earthquake history, 7. Present-day crustal movements and the mechanics of cyclic deformation: 8. Lithospheric structure and tectonics from seismic-refraction and other data: 9. Crustal and lithospheric structure from gravity and magnetic. The late Cretaceous granitoids of the Old Woman Mountains in the Mojave Desert, California, provide an excel-lent opportunity to apply these analytical techniques.
The peraluminous granites of the Sweetwater Wash, Painted Rock, and North Piute plutons represent different depths of the magmatic system, and are well understood in terms. SEISMICITY AND SEISMIC HAZARDS 4.
The assessment of seismic'haiards at Yucca Mountain focuseson characterizing the potential vibratory ground motion and fault displacement tha.About U.S., School Yearbooks, This is an indexed collection of middle school, junior high, high school, and college yearbooks from across the United States.
Yearbooks are one of those home sources, usually found in an attic or basement, which many people don't think of as a family history source.expeditions did not report this tiny bird anywhere in the eastern Mojave Desert.
Of the few sites from which Joseph Grinnell and Alden Miller cited it in their book on the distribution of California birds, the highest in elevation is Goffs, at feet. We have recorded the Black.